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Journal Article

Aspects of relationships between deformation and prograde metamorphism that cause evolution of water.

Metamorphic Reactions: Kinetics, Textures, and Deformation (1985) 211-241
DOI: 10.1007/978-1-4612-5066-1_8
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Abstract

Experimental observations of a sharp change in rock strength when the sample (serpentinite, gypsum, chlorite) dehydrates are used to evaluate the geological significance of elevated pore pressure, especially as regards changing style of deformation. -R.A.H.

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Murrell, S. A. F. (1985). Aspects of relationships between deformation and prograde metamorphism that cause evolution of water. Metamorphic Reactions: Kinetics, Textures, and Deformation, 211–241. https://doi.org/10.1007/978-1-4612-5066-1_8

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